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	<title>Silchhari, The - Revision history</title>
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	<updated>2026-04-21T17:47:29Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<title>0:0:0:0:0:0:0:1: Content Updated.</title>
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		<updated>2021-06-17T19:35:21Z</updated>

		<summary type="html">&lt;p&gt;Content Updated.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Silchhari, The&amp;#039;&amp;#039;&amp;#039;  a tributary stream of [[Karnafuli River|karnafuli]] river. It originates in the northern part of the Sitapahar anticline. Rocks of the Bhuban Formation are exposed here. The stream is about 1.3 km west of Kaptai along the Kaptai-Chandraghona road. At the mouth of the stream a miniature delta has been formed. In the middle of the stream lateral erosion and deposition took place on the beds. Here the stream has a gentle slope and meanders, which is the evidence of the mature stage of the stream. At a distance of about 290m there are a series of successive [[Waterfall|waterfall]]s, called rapids. The most prominent rapid of seven steps is at a distance of about 335m upstream. These rapids caused by a relatively resistant bed of [[Sandstone|sandstone]] are underlain by beds of nonresistant shales. At the source of the stream the most prominent waterfall with a vertical fall of about 15.25m occurs. [Sifatul Quader Chowdhury]&lt;br /&gt;
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[[Category:Natural Sciences]]&lt;/div&gt;</summary>
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